Sifonoforos (Cnidaria, Hydrozoa) De Aguas Superficiales Alrededor De La Isla Santa Clara, Durante Septiembre Y Noviembre Del 2007

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Sifonoforos (Cnidaria, Hydrozoa) De Aguas Superficiales Alrededor De La Isla Santa Clara, Durante Septiembre Y Noviembre Del 2007 ACTA OCEANOGRÁFICA DEL PACÍFICO. VOL. 17, N° 1, 2012 SIFONOFOROS (CNIDARIA, HYDROZOA) DE AGUAS SUPERFICIALES ALREDEDOR DE LA ISLA SANTA CLARA, DURANTE SEPTIEMBRE Y NOVIEMBRE DEL 2007 Por. Carlos Andrade1 RESUMEN Se analizaron los sifonóforos colectados en las muestras superficiales de zooplancton alrededor de la Isla Santa Clara durante septiembre y noviembre de 2007, identificándose 15 especies de sifonóforos del suborden Calycophorae y una especie del suborden Cystonectae, todos ellos registrados por primera vez para aguas tropicales al rededor de la Isla Santa Clara. Las especies más abundantes en la fase de flujo fueron Muggiacea atlantica (15.3%), Chelophyes appendiculata (13.3%) y en reflujo fueron Chelophyes appendiculata con 22.6%, Lensia hotspur con 15.5%, Diphyes dispar (11%) y Lensia multicristata con 10.9%. Las especies restantes fueron escasas y su abundancia relativa fue inferior al 8%. Palabras claves: sifonóforos, zooplancton, abundancia, Isla Santa Clara, biomasa. ABSTRACT We analyzed the collected siphonophores in surface samples of zooplankton around the island of Santa Clara in september and november 2007, identifying 15 species of the suborder Calycophorae and one species of suborder Cystonectae, all recorded for the first time in tropical waters around of the island of Santa Clara. The most abundant species in the flow phase were Muggiacea atlantica (15.3%), Chelophyes appendiculata (13.3%) and reflux were Chelophyes appendiculata with 22.6% with 15.5% Lensia hotspur, Diphyes dispar (11%) and Lensia multicristata with 10.9%. The remaining species were scarce and their relative abundance was less than 8%. Key words: siphonophores, zooplankton, abundance, Santa Clara Island, biomass. (1) Instituto Oceanográfico de la Armada. Casilla 5940. Av. 25 de Julio vía Puerto Marítimo, Base Naval Sur Guayaquil, Ecuador. Email: [email protected] 139 Sifonoforos (Cnidaria, Hydrozoa) de aguas superficiales …. Carlos Andrade INTRODUCCIÓN distintos y funcionalmente especializados. Se distinguen de los otros hydrozoa por presentar El conocimiento del plancton de la Isla Santa los dos estadios, polipoides y medusoides, en la Clara es extraordinariamente reciente y se misma colonia sin alternancia de generaciones limita a algunas colectas de organismos (Pugh 1996). planctónicos realizadas en monitoreo en los últimos diez años. Viven desde pocos meses hasta más de 10 años (Pugh 1996). Son bioindicadores de las Los sifonóforos constituyen uno de los grupos condiciones hidrológicas asociadas a las más importantes dentro de las poblaciones principales regiones climáticas y masas de agua planctónicas al formar parte de la cadena de (Alvariño 1981, Véliz 1981, Thibault-Botha et alimentación dentro del segundo nivel trófico, al. 2004) y establecen asociaciones simbióticas algunas de las especies más grandes se muy importantes con gran variedad de alimentan de peces (Trogouboff, 1957). organismos hasta relaciones de mutualismo y parasitismo (Pugh 1996). Los estudios del zooplancton e ictioplancton alrededor de la isla son escasos y esporádicos. En general los sifonóforos se distribuyen en Cajas et al., (1997 a-b-c y 1998), realizaron todos los océanos, mares y bahía, a lo largo de estudios del fitoplancton y zooplancton en el la columna de agua hasta los 4500m de entorno de la Isla. profundidad, aunque cada especie puede habitar intervalos de profundidad diferentes, Ortega y Calderón (1997), realizaron estudios y estando restringidas algunas a aguas cálidas reportaron huevos y larvas de peces en la zona superficiales (Pugh 1996). La mayoría de las adyacente de la Isla Santa Clara, durante junio especies habita el cinturón trópico-ecuatorial; hasta agosto 1997. una bución, y sólo un número limitado es exclusivo de altas latitudes (Alvariño 1981). Jiménez (1997), Cevallos (2006), determinó la Existen algunas especies con afinidades por abundancia de los principales grupos aguas neríticas costera, pero siempre son zooplanctónicas en la Isla Santa Clara. Sin encontradas en aguas donde la salinidad no es embargo, es preciso determinar las especies muy diferentes a la del agua de mar. Entre planctónicas presentes en sus aguas para tanto, la mayoría es típicamente oceánica (Pugh conocer la biodiversidad acuática de la zona. 1996). Por esta razón se ha considerado el estudio de los sifonóforos, por ser uno de los componentes Los sifonóforos pueden estar directamente rela- importantes del plancton gelatinoso, oceánico cionados con las zonas de frente (estacionales e de aguas cálidas y tropicales. intermitente) (Grahan et al. 2001). Y debido a sus características es probable que sean parte Los sifonóforos fueron descritos por primera del grupo de especies que se benefician con vez a fines del siglo XVII. Sus representantes esos eventos. poseen el mayor grado de polimorfismo y especialización funcional y una compleja A pesar de la existencia de información organización colonial (Dunn 2005b). Podemos relevante sobre sifonóforos (Gasca 2002), la definirlos biológicamente como colonias mayor parte de ésta se relaciona con la formadas por zooides asexuados genéti- taxonomía, mientras que muy pocos estudios camente idénticos, pero estructuralmente fueron relacionados sobre la ecología, 140 ACTA OCEANOGRÁFICA DEL PACÍFICO. VOL. 17, N° 1, 2012 desarrollo y organización de las colonias de la Isla Puná, es el principal estuario del (Haddock 2004). Pacífico Sudeste, componente hidrográfico de alta productividad biológica (Stevenson, 1981), La diversidad de especies en el océano cambia influenciada por la corriente de Humboldt en con la latitud, la longitud y la profundidad, diferentes intensidad de acuerdo a la época del pudiendo seguir determinados patrones que son año, dicha zona es considerada reserva conocidos para pocos grupos de invertebrados biológica y punto estratégico que sustenta las y para ciertas regiones de los océanos, pesquerías industriales y artesanales, en un área generalmente fuera de los trópicos (Witman & cuyo promedio de profundidad oscila entre 6 a Roy 2009). 20 metros correspondiente a la Ecoregión Marina Guayaquil y región tumbesina, la isla La presente investigación tiene como objetivo Santa Clara y sus alrededores constituye unos determinar la composición específica de los de los refugios más importantes de la costa sifonóforos colectados en aguas superficiales ecuatoriana por albergar grandes concen- entorno a la Isla Santa Clara y que permitan traciones de aves marinas, principalmente aportar con nuevos conocimiento de la fragatas, pelícanos y piqueros patas azules, diversidad planctónica en esta reserva además el refugio fue designado como humedal biológica. Ramsar en el año 2002 por desempeñar un papel primordial como indicador de calidad ÁREA DE ESTUDIO ecológica y bilógica de la Isla ECOLAP y MAE. 2007. (Figura1). La isla Santa Clara, también denominada como Isla del Muerto, (3º10’13’’ S. y 80º26’11’’ W), El estudio se realizó en 11 estaciones de está ubicada en la parte central del Golfo de monitoreo, realizados en los meses de Guayaquil, aproximadamente a unos 45 Km. al septiembre y noviembre del 2007 en la zona oeste de Puerto Bolívar y a 25 Km. al suroeste adyacente a la Isla Santa Clara. Figura.- 1 Ubicación Geográfica de las estaciones de monitoreo en la Isla Santa Clara, durante los meses de septiembre y noviembre del 2007. 141 Sifonoforos (Cnidaria, Hydrozoa) de aguas superficiales …. Carlos Andrade MATERIALES Y MÉTODOS RESULTADOS. Las condiciones térmicas y salinas en el área de Los resultados del presente estudio se basaron estudio fueron muy homogénea, observándose en el análisis de las densidades poblacionales para el mes de septiembre una temperatura de los sifonóforos colectados de las muestras media de 22.02ºC y 33.17 ups, mientras para el tomadas entre septiembre y noviembre del mes de noviembre se reportó una temperatura 2007. de 23.63ºC y salinidad de 33.7ups. En las muestras analizadas se identificaron 15 Los arrastres superficiales se los realizaron especies de sifonóforos, todas pertenecientes al durante 5 minutos a una velocidad de 2 nudos a suborden Calycophorae y una especie del bordo de una embarcación de fibra con motor suborden Cystonectae. fuera de borda de 75 HP. Abundancia relativa de las especies de Todas las muestras biológicas fueron obtenidas Sifonóforos durante las fases de flujo y con red Cónica Simple (WP-2) con apertura de reflujo, durante septiembre y noviembre de malla de 335µ y diámetro de la boca de red de 2007. 0,30m. El volumen de agua filtrada se lo En forma general en toda el área de estudio se obtuvo siguiendo las fórmulas establecidas por determinó cuatro especies dominantes en fase Boltovskoy 1981, los datos obtenidos fueron de reflujo, Chelophyes appendiculata (22.6%), extrapolados a (100m3)-1. Lensia hotspur (16%), Diphyes dispar (11.1%) Las muestras colectadas fueron tratadas con y Lensia multicristata con 10.9%. Mientras en cloruro de magnesio como narcotizantes de los fase de flujo se determinaron dos especies organismos gelatinosos y luego fijados con dominantes, Muggiacea atlántica (15.3%), formalina al 4% y neutralizado con bórax Chelophyes appendiculata (13.3%), Sin (Boltovskoy, 1981). embargo para el mes de noviembre en fase de flujo se determinó tres especies dominantes, Para la identificación taxonómica de los Diphyes dispar (33.5%), Sphaeronectes sifonóforos se siguió las claves de Boltovskoy, gracilis (16.4%) y Lensia subtilis con 10.57% 1981, Tregouboff, G. & M. Rose (1957); Pugh. de su abundancia. En fase de reflujo se reportó (1999), Totton
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